SFShao-Hua Fang

Shao-Hua Fang

*This is an algorithmically generated author record based on publicly available information.

Current Organizations / Institutes

The organizations/institutes from the scholar's latest article


Shao-Hua Fang has a total of 4 co-authors. Here are the top co-authors by number of shared publications:

  • Huan-Yu Liao

    Institute of Palaeontology; Yunnan Key Laboratory of Earth System Science; Yunnan University; Kunming 650500; China

    3 shared publications
  • Zhuo Feng

    State Key Laboratory for Vegetation Structure, Functions and Construction (VegLab), Institute of Palaeontology, Yunnan Key Laboratory of Earth System Science, Yunnan University, Kunming 650500, China

    2 shared publications
  • Di-Ying Huang

    Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences 1

    1 shared publication
  • Jian Gao

    State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China

    1 shared publication

Latest Publications

  • Open Access

    Revising some fossil clam shrimps (Branchiopoda: Diplostraca: spinicaudata) from the Upper Triassic in Yunnan Province and chongqing city, southwestern china

    by Shao-Hua Fang, Zhuo Feng, Huan-Yu Liao

    Abundant Triassic spinicaudatans from China have been commonly assigned to the genus Euestheria Depéret & Mazeran. However, recent SEM-based studies have revealed that many of them do not belong to euestherids, as evidenced by their distinctive micro-ornamentations, revealed by scanning electron microscopy (SEM). In this study, we describe two spinicaudatan species, Polygrapta yipinglangensis comb. nov. and P. dazuensis comb. nov., which were previously identified as members of Euestheria from the Upper Triassic Ganhaizi and Xujiahe formations in south-western China. The carapace ornamentations of these species exhibit fine polygonal reticulations in the upper parts, which gradually transform to linear arrangements and radial lirae at the ventral regions. Based on these features, they are classified into Polygrapta Novojilov. Although the two species exhibit morphological similarities, they can be distinguished by variations in reticulation size and the width of linear arrangements in their marginal areas.


  • Open Access

    A Worldwide Annotated Checklist of Fossil (Devonian–Cretaceous) Species of the Clam Shrimp Genus Euestheria (Branchiopoda: Diplostraca: Spinicaudata)

    by Shaohua Fang, Huanyu Liao

    Clam shrimps are one of the most common and representative invertebrates in continental strata and are endowed with important biostratigraphic and paleoecological values. The genus Euestheria is one of the most common clam shrimp taxa that has been recorded in the latest Paleozoic and the Mesozoic around the world. A list of all the species assigned to Euestheria, recorded from the Devonian to the Cretaceous across all seven continents as of September 2024, is provided. The list may serve as a valuable resource, potentially useful for the biostratigraphic division and long-range correlations of continental strata. In addition, the taxonomic issues of the genus are briefly introduced and examined herein. The study aims to provide a simple lead-in for all the researchers who have an interest in clam shrimp and the genus Euestheria.


  • A new clam shrimp (Branchiopoda: Diplostraca: Spinicaudata) from the Upper Jurassic in the Jiyuan Basin, China and its biostratigraphic significance

    by Huan-Yu Liao, Shao-Hua Fang, Zhuo Feng, Jian Gao, Di-Ying Huang

    A new spinicaudatan species Triglypta jiyuanensis Liao & Huang sp. nov. is described from the Upper Jurassic Maao Formation in the Jiyuan Basin, northwestern Henan Province, China. The carapace of the new species is ornamented with punctae, linear arrangements of punctae, and radial lirae. The new species differs from those of the early Triglypta forms from the Middle Jurassic but closely resembles T. jianchangensis Wang, 2014 from the Upper Jurassic Tiaojishan Formation of western Liaoning Province. Our study provides new biostratigraphic evidence supporting that the Maao and Tiaojishan formations can be correlated. Moreover, we suggest that the Yangshuzhuang Formation in the Jiyuan Basin could correlate to the Haifanggou and the Longmen formations in the Yanliao area.